9th Grade Chapter 3 Lesson 5

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Meteorology ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]

Meteorology ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]

Meteorology ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]

Meteorology ,[object Object],[object Object],[object Object],[object Object],[object Object]

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thermodynamics dew point lab report Generally, hygrometers, or cooled mirrors, have been the conventional air measurement tools used for precise dew point measurement. The device is considered to be a humidity transfer standard. The process entails cooling a mirror until water vapor begins to condense on the surface. The temperature of the mirror is measured. This projects the dew point of the air. This process is generally used in laboratory practices. A dew-point hygrometer was invented in 1751. For this instrument, cold water was added to water in a vessel until dew formed on the vessel, and the temperature of the vessel, the dew point, provided a direct index of humidity. In this experiment acetone is used even though the sample is not necessary to be acetone nor the amount of volume matters that becomes vapor so that the temperature (dew point) is measured until the metal mirror starts to condense. . Relative Humidity Relative humidity (RH) is the ratio between saturated humidity over absolute humidity at a given temperature. Relative humidity depends on temperature and the pressure of the system of interest. It requires less water vapor to attain high relative humidity at low temperatures; more water vapor is required to attain high relative humidity in warm or hot air. Relative humidity is normally expressed as a percentage ; a higher percentage means that the air water mixture is more humid ; a lower percentage means that the air-water mixture is less humid. Relative Humidity (%RH) =𝑭𝑺𝐅𝐀∗%𝟏𝟎𝟎 Absolute humidity is the total mass of water vapor present in a given volume of air. It does not take temperature into consideration. Absolute humidity in the atmosphere ranges from near zero to roughly 30 grams per cubic meter when the air is saturated at 30 °C (86 °F). Finding Dew point by hygrometer 4 Absolute humidity is the mass of the water vapor divided by the volume of the air and water vapor The absolute humidity changes as air temperature or pressure changes. The saturation humidity (Hs or FA) is the maximum quantity of water vapor that air can contain at a given temperature, without phase separation. The relative humidity (φ or RH) is the ratio (as percentage) of the partial pressure of water vapor in air, to the vapor pressure of liquid water at the same temperature. phase change occurs at dew point temperature when the temperature of a gas is the temperature at which the water vapor or low-boiling hydrocarbon derivatives contained in the gas is transformed into the liquid state. The boiling point of a liquid varies according to the applied pressure; the normal boiling point is the temperature at which the vapor pressure is equal to the standard sea-level atmospheric pressure (760 mm [29.92 inches] of mercury). At sea level, water boils at 100° C (212° F). Finding Dew point by hygrometer 5 Physical bases of the Measurement Procedure: At room temperature ether is close to its boiling point. Rapid evaporation is already taking place

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